anejo 5.1 especificaciones para construcción en Áreas propensas a terremotos dia- p gasoducto
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ANEJO 5.1
Especificaciones para Construccin en reas Propensas aTerremotos
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Seismic Design Work by Gulf Interstate Engineering Company
Design Projects by GIE:
1. Reliance Pipeline (India): Design of fault crossings (2006)
2. Southwest Products Pipeline (China): Design of fault crossings (2002)
3. PG&E Gas Pipeline (California): Design of fault crossings (1991)
4. Nikiski Products Pipeline (Alaska): Design of pipeline including fault crossings (1977)
Projects which GIE Provided Seismic Design Criteria and Procedures:
1. Southwest Products Pipeline (China): Developed design criteria and procedures
necessary for the pipeline to accommodate the effects of seismic activities, includingseismic shaking, pipeline stability in liquefiable soil, landslide, and fault crossings (2002).
2. Northwest Alaska Gas Pipeline (Alaska): Developed design criteria and procedures
necessary for a Trans-Alaska gas pipeline to accommodate the effects of seismic
activities, including seismic shaking, pipeline stability in liquefiable soil, landslide, and fault
crossings (1977-1980).
Projects which GIE Reviewed and Approved Seismic Design by Others:
1. Camisea Pipeline (Peru): Design for landslides by TECHINT (2004)
2. Camisea Pipeline (Peru): Design for fault crossings by ABS Consulting (2002)
3. ENRON MetGas Pipeline (India): Design for fault crossings by ENGINEERS INDIALIMITED (2002)
4. Alyeska-Trans Alaska oil Pipeline (Alaska): Pipeline Design for seismic activities,including fault crossings, seismic shaking, and slope stability for U.S. Department ofTransportation (1976 & 1977)
Mitigation measures taken in design Pipeline in Earthquake Prone Areas:
Rerouting the pipeline to avoid the problem area.
Realigning the pipeline across a fault to ensure that the pipeline remains in tension duringany seismic activity,
Burying the pipeline in a wide ditch with long side slopes and backfilled with compactedsand to allow for lateral deformation of the pipeline alignment.
Ensuring that the pipeline has sufficient bends in the line to allow flexibility.
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Known Occurrence of Seismic Activities:
Camisea Pipeline (Peru): Sustained a 9.7 earthquake in 2007 with no damage topipeline.
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1.0 DESIGN FOR EARTHQUAKES AND GROUND DEFORMATIONSEarthquake damage to buried pipelines may be divided into two categories: (1) stress and strain
induced during transient seismic wave propagation and (2) stress and strain induced by
permanent ground deformation (PGD). Permanent ground deformations include surface faulting
and other ground movements which may be triggered by transient ground shaking during
earthquakes, including landslides on slopes, mudslides, or liquefaction of saturated sand. Faultsand landslides are likely to impose high levels of stress and strain in buried pipelines. Soil
liquefaction may cause lateral spreading of soil and/or flotation of the buried pipeline if notproperly weighted.
The principal failure modes of continuous pipelines buried at least 1 meter deep include tensilerupture and local buckling. Pipelines buried less than 1 meter deep may experience beam
buckling. Beam buckling has also occurred during post-earthquake excavation to relieve
compressive stresses
2.0 STRESS AND STRAIN CRITERIA FOR EARTHQUAKE LOADSASME B31.8 and other pipeline design standards place limits on the allowable pipe stresscaused by internal pressure and other primary design loadings, including dead loads, live loads,thermal effects and outside forces. These limits are a percentage of the specified minimum yield
strength of steel. For contingent seismic events, the pipeline may be designed based on a strain
criteria, as allowed by ASME B31.8,833.5. This criteria is intended to prevent failure of thepipe and limit unacceptable damage. Even though an earthquake or landslide may not cause the
pipe to fail, it is important to inspect the pipe for damage or deformation after such an event
before the pipeline is placed back into operation. Pipe containing unacceptable deformationmust either be repaired and/or replaced.
Pipe response to active fault movements and other seismically induced ground considers the
forces of pipe-soil interaction, large-scale deformation of pipe, and elasto-plastic pipe material.
Two failure modes are considered, tensile rupture and local buckling (wrinkling).
3.0 TRANSIENT WAVE PROPAGATION
When seismic waves travel along the ground surface, any two points located along the
propagation path will undergo out-of-phase motions. These motions induce both axial andbending strains at the pipe-soil interface of a buried pipeline. In a buried pipe the stresses due to
seismic wave propagation depend on the friction angle between the soil and pipe, the soil
subgrade modulus, seismic shear wave velocity, and the period of the earthquake wave.
Analytical studies as well as buried pipeline performance during past earthquakes have shownthat transient seismic wave propagation is unlikely to cause direct damage to modern X-grade
pipelines with quality welds. For most soils, simplified calculations will determine that stressand strain are within acceptable limits
The compression waves may cause beam buckling in a pipeline if there are sharp, small radius
bends in the pipeline and the pipe is buried less than 1 meter deep. However, buckling isunlikely to occur at the large radius field bends that are used in this pipeline.
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4.0 PIPELINE STABILITY IN LIQUEFIABLE SOIL
Ground shaking during earthquakes may cause the transformation of a saturated cohesionless
soil from a solid to a liquid. In this state, the soil behaves like a heavy fluid. This may result in
substantial deformation of the pipeline by means of buoyancy, subsidence, or loss of bearing.
For liquefaction to occur, the grain size of saturated soil must range from 0.02 mm to 2.0 mmPipeline flotation or subsidence in itself would not necessarily cause the pipeline to rupture, but
it would create service or maintenance problems. However, excess stress and strain may becaused at the locations of abrupt transition from liquefied to stable soil. Identification of areas
that will liquefy must be based on site conditions, earthquake intensity and soils drilling data.
Studies should be undertaken along the pipeline route to identify areas where liquefaction islikely to occur. The pipeline should be re-routed around these areas where possible. Where it is
not possible to avoid these areas, the design should consider the pipe stress at the transition
zones and/or modify the design to mitigate and minimize the damage that may occur. Concepts
that may be considered are as follows:
deeper burial of the pipe to a level below the liquefiable soil,
shallow burial near the transition from stable to liquefiable to reduce differential
movement,
an above ground support system with deep foundations extending into the stable soil,
soil stabilization where the extent of liquefiable soil is limited,
additional pipe weight to prevent flotation or intermittent pipe anchors to resist uplift
forces, and
installation of automatic shut-off valves on each side of the liquefiable soil area
5.0 DESIGN OF ACTIVE FAULT CROSSINGS
The characteristics of an active fault include type of fault, direction of movement, amount of
movement, and zone of influence. For example, Figure 1 demonstrates a strike-slip fault with a
horizontal displacement ( s) and a crossing angle beta ( ) less than 90 degrees. The fault
shown is a right (dextral) moving fault that will cause tension in the pipe. Note that the beta ( )angle is measured counter-clockwise from the fault line to the pipeline. If the fault were a left
(sinistral) moving fault, the configuration would cause compression in the pipe, and beta ( )angle as used in the analysis would be measured clockwise from the fault line to the pipeline
(i.e. greater than 90 degrees).
The design of each active fault crossing is based on a combination of the following elements:
1) Specify the fault crossing intersection angle beta ( ). This angle must be maintainedthrough the zone of influence and for a length greater than the length of curve on
both sides of the zone of influence.
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2) Design of a special trench configuration through the zone of influence of the fault
and for a length of the curve on both sides of the zone of influence. The trenchconfiguration is designed to facilitate the lateral movement of the pipe.
3) Control the type of backfill and compaction of backfill in the special trenchconfiguration to limit the bending strain in the pipe.
4) Control of type and compaction of backfill in the standard trench for the total
affected length on each side of the zone of influence. This controls the axial soilrestraint of the pipe to allow elongation over the full affected length and thus reduce
the total percent of axial strain.
Fault
Pipeline
(a) Before Fault Movement
Deformed Pipe
(b) After Fault Movement
Figure 1: Simplified Model for Pipeline Crossing Strike-Slip Fault
The final design may be based on selecting a combination of crossing angle and type of soil to
be used for controlled backfill. The strain induced at a fault crossing may also be decreased byincreasing the pipe wall thickness
As an alternate design for crossing faults which cannot be aligned properly or which
special trench and controlled backfill is not desired, the pipeline may be installed above
ground within the fault crossing zone of influence, and placed on concrete supported,
steel supports. The design must provide sufficient flexibility so that the pipeline can
sustain the fault displacement without exceeding the allowable stress and strain.
s
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6.0 LANDSLIDES AND MUD SLIDES
The type of soil and its stability must be determined in areas where it is planned to
install the pipeline on mountain slopes or any other areas that may be susceptible tolandslide or mudslides.
Detailed design of the pipeline must consider site specific static and dynamic analyses
for failure. A preliminary assessment of potential problem areas should be made. If theresults indicate a potential for landslides, detailed engineering design must consider site
specific static and dynamic analyses for failure. Some of the techniques for preliminaryassessment include the following:
Survey of case records of slope failures and collection of data from other sources
Field reconnaissance surveys by experienced personnel to identify slopes requiringdetailed analysis.
Use of photogrammetric or other surveying methods to identify slopes steeper thana specified gradient.
Preliminary analysis using conservative design parameters and analytic technique toidentify potentially unstable slope along the alignment so that detailed analysis can
be limited in number.
Unstable areas should be avoided by pipeline re-routing, if at all possible. Wherecrossing unstable areas is unavoidable, the following concepts may be considered for
risk mitigation.
Direct mitigation of the problem area, if economically feasible.
Orienting the pipeline so that the pipe axis is parallel to the direction of groundmovement Deeper burial of the pipe to a level below the unstable soil.
Modification to the construction zone and trench configuration.
Using heavier wall pipe for added strength.
Using tunneling or horizontal directional drilling (HDD) at the crossing to place thepipeline in stable ground underneath the unstable area (for use in any unstableground).
The most appropriate design solution to remedy the unsatisfactory conditions will vary
from slope to slope. This will depend not only on the geotechnical factors involved, butalso on civil/pipeline design and construction consideration and environmental,
drainage and erosion concerns.
Direct mitigation concepts are as follows:
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Grading to flatten slopes,
Provisions for subsurface drainage paths,
Soil densification and stabilization,
Replacement of susceptible soil,
Grouting or chemical stabilization,Slope buttressing or construction of retaining walls,
Installation of automatic shut-off valves on each side of the hazardous area, and
Close monitoring of the areas by aerial patrol and ground reconnaissance for earlyidentification and mitigation.
For most areas with potential landslide hazards, stabilization and/or repairs will not be
cost effective or practicable. For many areas, improving surface drainage and periodicmonitoring may be more effective.
7.0 KARST AREAS
The pipeline passes through terrain underlain by rock where karst processes create cave
caverns and sinkholes. These processes are the result of long term dissolution of solublecarbonate rock by slightly acid ground water and underground streams. The majorhazards to a pipeline in karst areas is the development of sinkholes which causes a loss
of support underneath the pipe so that it spans the extent of the sinkhole. If the diameterof the sinkhole is greater than the allowable span of the pipe, the pipe will be over
stressed and may fail.
Three major types of sinkholes may occur:
solution sinkholes,
cover-subsidence sinkholes, and
cover collapse sinkholes.
Solution sinkholes form in areas where carbonate rock is exposed at the ground surfaceor is thinly covered by permeable sediments. These sinkholes generally form by a
gradual downward movement of the ground surface and development of a depressionthat is typically bowl shaped and shallow. This type of sinkhole is not likely to damage
the pipeline since the pipe can settle to conform to the curve. In addition, such adepression should be detected by regular pipeline surveillance before it has developed
to an extent that it has caused damage to the pipeline.
Cover subsidence sinkholes occur in areas where carbonate rock is covered by relativelynon-cohesive and permeable unconsolidated sediments As the underlying carbonates
dissolve, individual sediment grains move downward in sequence to occupy spaceformerly occupied by carbonate rock. Sinkholes of this type are generally shallow, of
small diameter, and develop gradually. This type of sinkhole is not likely to damage the
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pipeline since the pipe can span small diameter holes. In addition, such a sinkholeshould be detected by regular pipeline surveillance and timely mitigation may be
undertaken.
Cover collapse sinkholes occur in areas where carbonate rock is overlain by sediments
with some degree of cohesion (e.g. sandy clays and clays). If a solution cavity in thecarbonate rock enlarges to such a size that the overlying material can no longer supportits own weight and collapses into the underlying cavity. Collapse is generally abrupt.
This type of sinkhole is most likely to cause damage to the pipeline.
Design of the pipeline to resist large, abrupt ground failures from cover collapsesinkholes is not practicable or feasible. It is recommended that the following approach
be taken:
make a geotechnical assessment to locate areas where collapse sinkholes areactively forming, and avoid these areas where possible,
locate any sinkholes that may be detected along the pipeline trench duringconstruction, and repair, and
regular surveillance for early detection during operations.
In order to assess the probability of pipeline failure due to formation of sinkholes, stressanalysis may be performed to determine the maximum allowable pipeline span lengths
to preclude overstressing the pipe steel. Such analysis should be based on pipediameter, pipe wall thickness, depth of pipeline burial in the area, and soil conditions.
The probability that an abrupt sinkhole of sufficient diameter to cause pipe failure
would form directly under the pipeline may be relatively low. This should bedetermined by a geotechnical assessment.
After construction, the Company should train its operation personnel to recognize the
early detection signs of possible sinkhole development, such as slumping or saggingobjects; structural failure or cracks in the ground surface; and/or unexpected ponding ofsurface waters. In the event that a sinkhole develops, appropriate site specific
mitigation measures should be undertaken.
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Typical Investigation Requirements for Seismic Design
1. Purpose of Geotechnical Investigation
To evaluate the pipeline route to determine geologic hazards to the pipeline,
including karst formations, fault crossings, ,slope stability and areas of potentialseismic induced ground failures such as landslides and liquefaction.
To provide recommendations regarding possible route refinements to avoidgeological hazards, or reduce geologic hazards; or design to accomadate the
hazards.
2. Karst Areas
Contractor shall identify areas along the pipeline route where existing sinkholes are
present and other areas which have a high potential for the formation of sinkholes.
Contractor shall also make recommendations for design to reduce the potential for
sinkhole.
2. Fault Crossings
Contractor shall identify active and potentially active faults crossed by the
pipeline and shall make design recommendations regarding the following:
Location of each fault along the pipeline route;
Width of the fault zone over which the surface displacement might occur;
Geometry of the fault relative to the pipeline;
Type, amount, and direction of fault movement that is likely to occur;
Recurrence interval for an appropriate seismic magnitude event along the
fault; and
Soils characteristics at the crossing and recommendations for soils design
values.
Bidder's proposal shall include a definition of the basic approach, types of
investigation, and proposed methods for identification and characterization of the
fault crossings.
3. Landslide Areas
Contractor shall identify areas along the pipeline route exposed to landslides
And shall make design recommendations regarding the following:
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Location and extent of each landslide hazard area along the pipeline route;
Recommendations for route alignment refinements to avoid or reduce the
effects of the landslide hazards;
Feasibility of stabilization of the landslide area;
Soils characteristics at the landslide area and recommendations for soils
design values.
Bidder's proposal shall include a definition of the basic approach, types of
investigation, and proposed methods for identification and characterization of the
landslide area.
4. Seismic Induced Ground Failures
Contractor shall identify areas along the pipeline route which have a high potential for
ground failures from slope instability, liquefaction, lateral spreading, andhydrocompaction resulting from seismic ground shaking. Contractor shall make
recommendations regarding the following:
Location and extent of each potential hazard area along the pipeline route;
Likelihood that ground failure hazards will occur in the hazard area;
Recommendations for route alignment refinements to avoid or reduce the
effects of the hazard;
Soils characteristics in the hazard areas and recommendations for soils
design values.
Bidder's proposal shall include a definition of the basic approach, the types of
investigation, and the proposed methods for identification and characterization of
the potential for seismic induced ground failures.
5. Final Report
The Contractor shall submit final reports detailing the work performed, observationsmade, results of laboratory and field tests, and the Contractor's recommendations for each
area of work, as applicable. Reports shall be submitted within 30 days of completion of
the geotechnical field investigations.
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Reports shall be in English, and using metric units of measurement. Terms used in the
final reports shall be in accordance with ASTM D653.
For each location investigated by the Contractor the following information shall be
presented:
description of location;
geomorphological characteristics, including but not limited to relative relief,
slope angle, and evidence of soil erosion;
soil mass characteristics if evident in areas of exposed soil;
geology, including tropical residual soil type;
hydrology, including drainage pattern, flow, and evidence of flooding;
vegetation, including broad type and percentage cover; and
dated photographs showing the typical features of the location.